Monday, May 15, 2017

New Gold Book Tells It All

As I continue to research my latest project - "Arizona Lode and Placer Gold - A Guide for Prospectors", I am amazed at all of the potential gold and silver deposits in Arizona. They are literally everywhere south of the Colorado Plateau province. And if anyone has a nose for finding gold deposits, I believe I'm one of those people.  I was harassed endlessly the last year before I retired from the Wyoming Geological Survey because a couple of democrats felt I was finding way too many gold, diamond and colored gemstone deposits in Wyoming.

I now have more than 300 pages of text in my Arizona book where I describe gold deposits, prospecting methods and provides information on hundreds of mines and prospects in Arizona and highlight some of the better prospects with GPS coordinates. 

So, if I can find so many good gold deposits, how come I'm not mining them? Well, first of all, I'm not a miner - I'm an explorer. Second, I don't have much money and it takes a lot of money to open a mine - and I hate staking claims - its boring. 

One  deposit I highlight in my upcoming book is the Taylor-Hermosa massive sulfide and replacement deposit in the Patagonia Mountains in southern Arizona. This is currently being developed into an underground mine with capitalization of $457 million, and it is not the only good deposit in the area. One deposit I assisted in discovery in 1988 in Alaska is one of the largest gold deposits on earth known as Donlin Creek. Last I heard, capitalization for this mine was $1.3 billion. But of course, these are giant mines - but there are many types of deposits of all different sizes. 

For me, I like the hunt - and there is no excitement in mining for me. So, instead of letting all of those great gold and silver deposits just sit around, I'm writing a book about them. I hope to have this book published by the end of 2017 - but watch this site for updates.

Saturday, October 29, 2016

Arizona's Mining Districts and Mines


Gold Basin District

Hey! Is that really Tony Beets? Nope, this is a dredge we visited in 1989 in Flat,
Alaska the year after our geology team with WestGold
  found one of the largestgold deposits in history at Donlin Creek, Alaska in 198
Many dry gold placers lie along the eastern edge of the White Hills and extend east to Hualapai Wash in Mohave County of northwestern Arizona (T28 & 29N, R17 & 18W). These are known as the Gold Basin placers. Get on your Google Earth and search for "Gold Basin, AZ" and hopefully, you will arrive in the middle of Gold Basin a short distance to the east and south of the many dry gold placers known in this basin.

The area lies south of Lake Mead, the Lake Mead Recreation area, and the Colorado River. The nearest communities are Meadview (36o00’00”N; 114o04’00”) and Dolan Springs (35o35’25”N; 114o16’25”W). Due to the large number of retirees and snowbirds settling in the region, each community is surrounded by extensive suburbs.

The placers are all dry placers in a desert, and these have detrital gravels that are only 1 to 5 feet thick that mostly lie on hard, false, bedrock of consolidated gravel cemented by caliche. The overlying gold-bearing gravels are weakly mineralized, and have considerable black sand and quartz with rock fragments of schist and gneiss eroded from the Precambrian terrain in the White Hills. 

The gold content of the placers is poor and may only be 0.03 to 0.04 ounce per cubic yard at best; while the underlying consolidated gravel remains unexplored. Gold nuggets are rare. Some up to an ounce have been found with the largest being only 4 to 5 ounces in weight (Nevada Outback Gems website). Much of the gold-bearing area is part of the White Mountains alluvial fan that extends from the eastern flank of the uplifted White Hills to Haulapai Wash to the east. The fan covers a surface area of 6 by 5 miles and you can drive to the area northward on the Pierce-Ferry highway (Road 25) through Dolan Springs. 

Lode gold was discovered in quartz veins in Precambrian rock in the 1870s. Placer gold from the veins was not found until the Great Depression. In 1932, W. E. Dunlop found gold in the dry gravel which attracted others. The amount of gold recovered by the prospectors was minor. Even experienced miners only made about $1 per day (1933 wages). And the total amount of reported gold recovered from the Gold Basin placers is only 415 ounces produced during the period of 1934-49.  To put this in perspective, this is equivalent to only one clean-up on Tony Beet's dredge in the Yukon!

The gold-bearing gravels occur in arroyos and gulches at elevations of 3,300 to 2,900 feet. The gravels have medium-grained, angular schist and gneiss fragments with a minor amount of finely divided quartz. A small number of boulders are encountered that are generally less than 2 feet in diameter. The gold occurs as flour gold and less commonly as angular nuggets with some gold attached to black schist particles. The White Hills, which are made up of granitic, schistose, and volcanic rocks, contain many argentiferous and auriferous quartz veins that are the likely source for much of the Gold Basin gold (Wilson, 1981).

The gold placers have erratically distributed gold. In addition to dry placer mining, there is considerable prospecting with metal detectors. Some find gold, while others have found a bonus of meteorite fragments (Nevada Outback Gems website).

Friday, August 31, 2012

United Verde Mines, Verde Distrinct, Jerome, Arizona

From Flagstaff, we decided to take a detour to the Verde district: a highly mineralized area. The district is 90 miles north of Phoenix along the edge of the Black Hills in Yavapai County, central Arizona and locally referred to as the Jerome district. It encloses a 30 mi2 mineralized terrain with two major mines along the northern edge of the town of Jerome. The two principal mines in the district are the United Verde and United Verde Extension. To get to the district, drive south on Highway 89A from Flagstaff. You can also visit the town on your computer by searching for “Jerome, AZ” with Google Earth.

On the northwestern edge of Jerome is a large, partially reclaimed, open pit mine that is part of the United Verde mine. The rest of the mine lies underground and inclues 81 miles of tunnels and shafts hidden beneath the open pit, Cleopatra Hill and the adjacent valley. A large active quarry is visible near the northeastern edge of town that is actually the Clarkdale quarry and cement plant, which has little to do with the base metal mines. Evidence of the old smelter works is visible further east near the Verde River and expressed as black slag with some old buildings and foundations.

If you are familiar with gossans, you should be able to trace an extensive belt of rusty-colored rocks on aerial photographs on Google Earth. I followed the gossan 7 miles north of the United Verde Mine, and another 7 miles south! Such an extensive gossan likely hides ‘blind deposits’! My experience is that for every mineral deposit found on the surface, there likely is many more hidden at depth in the immediate area (and who knows how many lie hidden under the adjacent valley sediments). And like most mines reported to have been mined out, the United Verde is far from being mined out. In fact, the US Geological Survey reported at least twice as much unmined ore remains in place as was mined in the past. Actually, it is extremely rare for a major mineral deposit to be mined out as most productive mines terminate operations because of declining economics as prices and markets fall during bad times.

Jerome, Arizona, looking towards Cleopatra Hill. The hill with the ‘J’ is
Cleopatra Hill and the United Verde open pit is the mine dump seen in
distance to the right of the J between the two prominent hills. The tops of
two head frames of the United Verde Extension mine are visible in the
When I was a student in geology, the Verde district was considered as an exploration model for ‘submarinevolcanogenic massive sulfide deposits’. One geological dictionary defines massive sulfide very simply as: “an unusually large deposit of sulfide minerals”. But there is more to massive sulfide deposits.

Massive sulfides bring thoughts of copper and zinc to geologists. And for myself, I also think of precious metals. Sulfide minerals in many of these can enclose significant amounts of gold and silver. So much silver was found associated with these deposits at Jerome that the recovered silver essentially paid for the mining operations. And many banded cherts (known as exhalites) associated with ‘submarine volcanogenic massive sulfides’ (VMS) contain anomalous gold.

VMS refers to a type of mineralization with zones of massive (as well as disseminated) sulfide minerals that were deposited beneath the ocean in hydrothermal vents including white and black smokers. Over geological time, many of these VMS deposits now lie on dry land due to tectonic forces while modern deposits continue to form under the ocean. Where found, VMS deposits are hosted in rocks 3.55 billion years old to the present and may even include deposits with a hundred million tons of ore rich in gold, silver, copper, zinc, lead and other metals.

White smoker sinter column. White smokers precipitate in hydrothermal
 vents and often have auriferous silica. Black smokers are sulfide rich
and associated with higher geothermal temperatures (specimen from the
United Verde mine, and on display at the Douglas Museum in Jerome).
VMS deposits have distinct rocks such as volcaniclastics (breccias) that represent very active submarine vents. Some of these are so distinct that one Canadian geologist dubbed them ‘mill rock’ years ago because he noticed there were operating mills and mines adjacent to many of these.

In addition to volcaniclastics (mill rock), siliceous mounds or chimneys are formed by submarine fumaroles that are referred to as black and white smokers. Other distinct rocks include layered stratiform rock known as exhalites that formed during eruption of heterogeneous volcanic material in sea water: the layering was produced by sea water naturally separating minerals by specific gravity as they slowly settled in the ocean water.

The host rocks for the VMS deposits in Jerome are 1.7 billion years old and similar in age to VMS deposits discovered in Colorado and Wyoming in 1979 and the early 1980s. You might be wondering what submarine VMS deposits are doing in the dry deserts of Arizona and high mountains of Colorado and Wyoming? In the geological past, these were accreted to continents and buried by tectonic forces related to continental drift. After millions of years of erosion following mountain uplift, some have been exposed at the surface, while many more remain hidden and undiscovered. Those hidden at depth are referred to as ‘blind’ deposits. Still others continue to form in the oceans, particularly along active volcanic island chains (such as Japan) and along spreading centers such as the Mid-Atlantic Ridge.

When I was the Senior Economic Geologist and Deputy Director at the Wyoming Geological Survey, Conoco Minerals discovered VMS deposits in 1979 in the Sierra Madre Mountains west of Saratoga. But few have heard of these deposits because of the US Forest Service. Those that were found near the old Itmay mine, not far from the famous Ferris-Haggarty mine, were withdrawn from public use. Other VMS deposits were soon found in Colorado and Wyoming. The discoveries sent shock waves through the Forest Service which had little taste for mining; and the agency hurried to withdraw the new discoveries until all, or portions or most VMS deposits fell within or adjacent to the withdrawals effectively locking out mining companies and prospectors from public land.

Much of this region in Colorado and Wyoming was known as the Grand Encampment district, which in the 19th century, prior to government interference, was a major base metal district. But because of the withdrawals, no jobs were created because of Conoco’s discoveries, no valuable metals were mined, and the US continued out-sourcing jobs and importing base metals.

Today, the Verde district is idle and the town of Jerome is a tourist attraction built on the flank of Cleopatra Hill which rises more than 6,000 feet above sea level. Some buildings in Jerome were constructed on the Precambrian rock that forms Cleopatra Hill, while the rest of the town slopes downward on Tertiary to Recent fanglomerates and landslide debris. The landslide has been a historical problem and periodically slides following periods of high runoff. At the base of the slope, the surface flattens eastward to the Verde River valley at Clarkdale and Cottonwood 4 to 5 miles east of Jerome at an elevation of 3,300 feet.

Jerome was a major copper-gold-silver-zinc-lead district. According to the Arizona Department of Mines and Mineral Resources (2007), 48 of 70 known VMS deposits found in Arizona have produced ore - all of which are Precambrian age (1.7 to 1.8 billion years old). Production from these totaled more than 55 million tons. Most of these deposits are steeply plunging and deformed, such as the United Verde, which has been described as a rod-like ore body or pipe located within an axis of a major, steeply-plunging, fold.

About 98% of the past production in the Verde district was from the United Verde and United Verde Extension mines. Even though mining ceased in 1953, there is evidence that the miners left behind considerable ore. The district was considered to be a copper district, but at today’s metal prices, the district would be classified as a copper-gold-silver-zinc district. Considerable copper, gold, silver with some zinc and small amounts of lead were recovered from the two principal mines.

In 1989, the US Geological Survey indicated records from Phelps Dodge showed production from the United Verde Mine from 1884 to 1975 amounted to more than 2,926,900,000 pounds ($10.1 billion at 2012 prices) of copper, 97,891,000 pounds ($82 million) of zinc, 459,000 pounds ($390 thousand) of lead, 49,603,000 troy ounces ($1.4 billion) of silver, and 1,354,200 troy ounces of gold. Koschmann and Bergendahl of the US Geological Survey reported gold production was even higher at 1,571,000 ounces ($2.5 billion) over the lifetime of the district.  Based on statistics from the U.S. Geological Survey and Phelps Dodge, the United Verde produced $14.8 billion in metals at 2012 prices.

High wall of the United Verde open pit mine with head frames in foreground. Note large distinct, rusty gossan produced by oxidation of massive sulfides in the background. The massive sulfides were so rich that they actually ignited and burned underground for many years!


The cupriferous gossan exposed at the surface at Jerome was found by prehistoric tribes hundreds of years ago. In 1875, the U.S. Army rediscovered the gossan and in the following year (1876) prospectors rushed to the district to claim the discovery. By 1882, much of the minable land had been consolidated by the newly formed United Verde Copper Company which began extracting near-surface oxidized and supergene enriched copper ore rich in gold and silver. Underground mining began in 1883, and open pit mining was initiated in 1920.

A second company, (United Verde Extension [UVX]), was organized in 1899 to search for a suggested, down-faulted continuation of the United Verde massive sulfide. UVX began searching southwest and east of the United Verde property. Their efforts were fruitless until they were on the verge of bankruptcy in 1914, when a drift driven from a shaft east of the United Verde mine intersected bonanza grade ore rich in chalcocite on the 1,200 level. In 1916, another ‘blind’ deposit was found. The ore was so rich the company ended the year with a 74% profit after expenses. Later geological studies showed the UVX discoveries were not part of an off-set of the United Verde ore body, but instead completely separate, ‘blind’ ore bodies.

The UVX mine operated on a large scale until 1938 when much of its high-grade was mined out and operations ceased. The nearby United Verde mine continued mining. After 1931, much of their activity focused on open-pit mining. Depletion of ‘high-grade’ reserves finally forced the mine to close in 1953. This resulted in many people reporting that the deposit was mined out. However, the operations left behind a giant, low-grade, ore deposit and who knows how many ‘blind’ deposits.

Banded Chert from the United Verde mine
The VMS erupted as hot, sulfide-rich material into cool water resulting in precipitation on the ocean floor 1.7 billion years ago. The Verde VMS lies at the top of a submarine rhyolite dome and flow breccia known as the Cleopatra Member of the Deception Rhyolite. The ore is zoned and capped by chert and siliceous massive sulfide that grades down into pyrite-rich massive sulfide, zinc-rich massive sulfide, copper-zinc-rich massive sulfide, chloritic stringer ore, and chloritized quartz porphyry ore. Gold is found throughout but is in greater concentrations at the stratigraphic top (siliceous massive sulfide and chert ore).

Gold is in greater concentrations in chert. For instance, on the 4500-foot level, the black schist yielded 0.002 opt Au and 0.71 opt Ag. In chert near the surface, the ore yielded values as high as 0.12 opt Au and 4 opt Ag (60 times more gold). On the 700-foot level, the massive sulfide averaged 10 times more gold than the black schist. A positive correlation of gold with higher zinc content was also recognized by the US Geological Survey. This is important as much zinc ore was not mined.

Sulfides are exposed at the surface down to the 4500-foot mine level, but in the geological past, the ore also extended upwards to the base of the Cambrian Tapeats Sandstone indicating at least 350 feet of vertical column of massive sulfide was removed by erosion. With this much erosion, drainages down-slope from the massive sulfide should contain detrital gold, but I could not find any report suggesting that gold had been detected in the nearby drainages. Based on the mode of occurrence, the gold would likely be very fine grained.

Ore minerals in the massive sulfide in decreasing abundance included pyrite, sphalerite, chalcopyrite, bornite, arsenopyrite, galena, tennanite and gold (electrum). Much of the electrum is thought to be present as microscopic inclusions in sulfide minerals. Silver is present in the electrum and in late-stage tennanite (Cu12As4S13) in quartz carbonate veins and in carbonate rich massive sulfide ore. The tennanite also contains gold as microscopic inclusions.

The Verde was the largest known volcanogenic massive sulfide deposit in the US with 33 million tons of mined ore, and 50 to 70 million tons of low-grade ore left in place. It is also considered to be one of the largest in North America. The massive sulfide was steeply-dipping, irregular- to cylindrical-shaped ore body approximately 700 to 800 feet in diameter that extended 2,400 feet deep. The United Verde mine reached a depth of 3,515 feet and included eight shafts. According to the US Geological Survey, proximal ore recovered from the mine averaged 4.77% Cu, 0.046 opt Au, and 1.65 opt Ag. Zinc and lead were not recovered during much of the operations. Another blind ore body was found in the lower levels of the mine 500 feet northwest of the roots of the main deposit.

Anomalous gold was detected in the pyritic and sphalertic massive sulfides and the chert rich ore: chloritic host rocks are poor in gold. The zinc ore contained as much gold as the copper ore. And because only the high-grade copper-rich portion of the massive sulfide lens was mined, a very large tonnage of low-grade ore remains in place and it was estimated that at least 75% of the mineralized deposit remains unmined because it was too low-grade to mine (<2% Cu) under historical economics. The estimates suggest about 115,000,000 tons of low-grade massive sulfide ore and 38,000,000 tons of mineralized black schist remain in the mine with grades of 0.5 to 1% Cu, 2 to 4% Zn, 0.01 to 0.015 opt Au and 0.5 to 1.0 opt Ag. This zinc-rich deposit is estimated to have 400,000 troy ounces of gold.

At the United Verde Extension Mine, mineralization occurred in an elliptical ore body hosted by the Deception Rhyolite and Grapevine Gulch Formation. The main chalcocite ore body was found on the 1400-level and was 269 feet wide and 440 feet long on this level.

You may not appreciate this exhibit at the Audrey Head-frame Park in Jerome if you have.
a fear of heights. Sunlight is projected down the 1900-foot deep Audrey shaft so visitors can
see the depth of these mines. When I took this photo, I was standing on the plexiglass
covering the deep shaft.

The UVX mine produced 3,879,000 tons of ore that averaged 10.23% Cu, 0.039 opt Au, and 1.71 opt Ag. Ore minerals included chalcocite, cuprite, native copper, malachite, chrysocolla and azurite hosted by felsic fragmental rocks, massive rhyolite and quartz porphyry – all units of the Deception Rhyolite.

Part of the UVX operation was developed by the Haynes Shaft due west the United Verde open pit. This deposit was another blind ore body found at 2,500 feet below the surface. The UVX decided to explore the ground under the Haynes shaft by driving a tunnel at the 3,000 level. A drift was started in 1930 and reached the Haynes massive sulfide pipe in 1931.

The Haynes proximal pipe was a steeply-plunging massive sulfide. It extended a short distance above the 2700-level downward to an undetermined point between the 3450 and 3700 levels of the United Verde Mine. The Haynes haft was sunk to 700 feet between 1907 and 1911; subsequently deepened to 1,200 feet, with 1,700 feet of drifts and crosscuts on the 700 level and 700 feet on the 1200 level.

Tuesday, January 10, 2012

Vulture Gold Mine, Arizona

Exposed gold-bearing gossan at the Vulture mine,
Vuture Mine. Gold was discovered 50 miles northwest of Phoenix in 1863 by Henry Wickenburg. The discovery led to the sinking of the Vulture mine shaft and development of an adjacent town named Vulture City. The town reportedly grew to a population of nearly 5,000. Today, Vulture City is a ghost town, but its ashes led the city of nearby Phoenix.

To visit the mine on Google Earth, search for ‘Vulture Mine, AZ 85390’ and this should take you 0.25 mile north of the mine. As you scan south, you will come across open cuts in rusty gossan at the mine site, remains of the ghost town to the east, the mill and assay office to the south of the gossan with extensive white leach pads.

The Vulture mine became known for high grade ore. History reports many people made a living from high-grading ore and those who were caught were hanged to stop theft at the mine (maybe similar opportunities provided to politicians and CEOs for high-grading public funds, taxes, and military secrets, would result in people who really represent our best interests).
Mine adit in fanglomerate at the Vulture
mine similar to many of Arizona's
 placer gold deposits.
Following discovery of gold, the precious metal was mined over the next three years from high grade ore milled in a primitive arrastre constructed to the east at the nearby Hassayampa River. In 1866, a 40-stamp mill was constructed on the Hassayampa River 12 miles to the northeast of the mine (other sources report the mill was a 20 stamp mill) and gold was recovered from high-grade ore reported to assay 1.2 to 4.5 opt Au. The mill site located at such a distance resulted in security problems: the ore had to be hauled by freighter wagon to the mill. And there are stories that suggest as soon as the wagons were out of site of the mine, high-grading was a common practice: so common that at least 18 men were hanged in Vulture City. Some suggest that freighting became more profitable than mining. In addition to high-grading by freighters, theft was common at the mill and by miners working underground.
In 1879, the mill was expanded to an 80-stamp mill. By 1888, the vein was lost along a fault contact on the 300-foot level and operations ceased. Twenty years later (1908), a comprehensive geological study led to discovery of the vein offset and the mine reopened and operated until 1917 when the vein was again lost along another fault.
View of the remains of Vulture City
behind gossan.

Exploration for the offset resulted in the sinking of a 500-foot shaft and the vein was rediscovered. The mine again operated until it was closed by a 1942 War Production Board order closing all non-essential gold mines in the US to ensure maximum effort was contributed to the war effort. Many mines that were closed at that time never reopened, suggesting that at today’s gold prices, many of these mines likely have commercial ore and potentially could be reopened.  The Vulture mine likely fits in this category; however, there is an effort to have the State of Arizona purchase the property for historic preservation, which would result in a valuable gold resource being preserved similar to the Carissa mine in Wyoming (like the Vulture, the Carissa mine was Wyoming’s largest historical gold producer and it was preserved by the State such that the gold resource is no longer available to the public: work by the author and past mining companies has shown the property likely has a very sizable gold resource that could be mined by open pit and underground [Hausel, 1991 and Hausel and Hausel, 2011]). The Vulture mine never reopened leaving one to wonder how much unmined ore and gold resources remain. The Vulture mine, the main incline shaft of the mine continues to a depth of 2,100 feet along a 35o incline.
Part of the ore zone at the surface of the Vulture mine -
highly silicified gossaniferous rock

A characteristic of much of the region in western Arizona is extensional faulting during the Miocene that produced numerous listric and planar normal faults. Such normal faults and associated fault blocks were rotated east to northeast and vein offsets are not uncommon.

The Vulture mine is surrounded by Miocene (23 to 5 million years old) andesites and rhyolites that lie unconformably on Proterozoic (2.5 billion to 600 million years old) schist and gneiss. These were tilted by rotational normal faulting such that the original bedding is now near-vertical to locally overturned, and faults exhibit gentle, westerly dips (Spencer and others, 1989).
Primary dipping vein at the Vulture.

Gold and silver were discovered in quartz veins and in silicified and altered host rock within and adjacent to a prominent north—northeast-dipping quartz-porphyry dike that intrudes Proterozoic basement rock and grades into a Late Cretaceous granite to granodiorite pluton to the west. The precious metal occurs in the form of native gold and electrum and is associated with sulfides including pyrite (fools gold), argentiferous galena (silver-bearing lead-sulfide) and minor chalcopyrite (copper-iron-sulfide) and sphalerite (zinc-sulfide). White (1988) reported a positive correlation of gold with abundance of secondary silica and sulfides. Pervasive wall rock alteration adjacent to the vein resulted in replacement of feldspar and mafic minerals to produce sericite, hematite and clay; thus the altered dike now consists of quartz ‘eyes’ in a fine-grained altered matrix. Gold is concentrated in quartz veins and in silicified and altered rocks within and adjacent to the dike.
Tightly folded Proterozoic basement
schist and gneiss exposed at the
mine site.
The mineralized zone is fault controlled and trends nearly parallel to foliation. The vein was traced for 1,000 feet and is 32 feet wide at the surface and swells to 47 feet on the 240-foot-level. To the west, the vein splits into smaller veins that are cut by several faults. Production figures are not complete, but the available reports indicate that the mine produced 340,000 ounces of gold and 260,000 ounces of silver from 1863 to 1942 from ore that averaged 0.35 opt gold and 0.25 opt silver (Spencer and others, 1989).  

The is a very interesting side to this mine. Apparently Jacob Waltz (known as the Lost Dutchman) worked at the Vulture mine for several years and legend suggests he likely high-graded considerable gold from the mine and his discovery of gold in the Superstition Mountains may actually be the gold high-graded at the Vulture (Miner, 1996-2011).
Today, the mine is inactive but the owners have made the available for self-guided tours for the public that are highly recommended.
Old headframe (right) with part of the exposed vein (left)
at the top of the hill
Just an interesting photo inside the assay lab.

Old assay furnace in the assay lab at the Vulture mine.
Old powerhouse at the Vulture gold mine.

Down Loadable Publications

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Minerals and Rocks

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